1.
Therefore, the CMB is the beginning and the end of whole mantle convection.
因此,地幔底层既是全地幔对流的起点,又是全地幔对流的终点。
2.
The issue of upper vs whole mantle convection is critically discussed.
最后,着重讨论了上地幔与全地幔对流的论争。
3.
Variable Viscosity Whole Mantle Convection and Surface Plate Motions;
全球变粘度地幔对流与地表板块运动
4.
The Numerical Modelling of Whole Mantle Convection and Its Geodynamic Implications;
全球地幔对流的数值模拟及其动力学意义
5.
In east pacific, however, the subduction direction of the subducting plate is the same as that of the flow of the mantle, so the current dip angle of the Benioff zone will be larger than the initial dip angle.
对地幔而言 ,则是地幔相对于地壳的东向流动。
6.
Numerical experiment is a basic method in the study of Earth's mantle convection.
数值实验是地幔对流研究的基本方法。
7.
Numerical Modeling of upper Mantle Convection and Orogeny of the Tianshan Mountains;
天山上地幔对流与造山运动数值模拟
8.
The Geological Evolution and Mantle Convection of the North China Platform in Early Precambrian
华北陆台早前寒武纪地质演化与地幔对流模式
9.
In mantle convection models, the mantle viscosity is generally assumed constant or dependent on depth.
粘度为常数或仅随深度变化是地幔对流模型中常用的假设.
10.
In this paper, recent developments which have heen made in the field of Earth's mantle thermal convection are critically reviewed.
本文着重介绍近年来关于地幔热对流模拟实验研究发展概况。
11.
Temporal Variation in Volume Flux of Hawaii Plume through 35 Ma
Hawaii地幔柱近35Ma的体积流量变化
12.
The theory of plate tectonics describes the motions of the lithosphere, the comparatively rigid outer layer of the Earth that includes all the crust and part of the underlying mantle.
板块结构理论描述岩石圈的运动。 岩石圈是相对坚硬的地球外层，包括全部地壳和部分地幔。
13.
Modeling experiment is an important method and the component part in the study of Earth's mantle convection.
模拟实验是当前地幔对流研究中的一个重要手段,一个重要组成部分。
14.
Upward mantle wedge convection recorded by Zhimafang orogenic garnet-lherzolite,Sulu UHP terrane,eastern China.
洋壳俯冲过程中的地幔楔上升对流:来自芝麻坊石榴子石二辉橄榄岩早期变质的证据
15.
The mesosphere comprises the rest of the mantle below the asthenosphere.
中间圈包括岩流圈以下地幔的其余部分。
16.
HELIUM ISOTOPIC EVIDENCE ON METALGENISIS OF MANTLE FLUIDS IN THE WANGU GOLD DEPOSIT, HUN AN PROVINCE
湖南万古金矿床地幔流体成矿的氦同位素证据
17.
The Chemical and Isotopic Compositions and Their Origin of Upper Mantle Volatiles in Eastern China;
中国东部上地幔不同类型流体组成及其性质
18.
The Petrographic and Petrochemical Characteristics of the Mantle Fluid Metasomatism;
地幔流体交代作用的岩相学和岩石化学特征